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      Expedition 362: Site U1481

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          Abstract

          Site U1481 (proposed Site SUMA-12A) is located on the Indian oceanic plate, east of the Ninetyeast Ridge, west of the North Sumatran subduction margin, and 35 km southeast of Site U1480. The primary drilling objectives at Site U1481 were (1) To core the deeper interval of the subduction input sedimentary section and basement; (2) To determine if the lower Nicobar Fan, pelagic section, and basement at Site U1480 are representative of this part of the Indian plate; and (3) To understand the degree of heterogeneity of sediment and basement over short distances. Specific objectives for this site include the following: (1) To establish the onset of Nicobar Fan deposition and to determine the primary sources of sediment delivered to the site during early fan history; (2) To identify the principal lithologies that may be involved in development of the plate boundary fault; (3) To establish how the mechanical/strength properties of the different lithologies change with depth to determine trends and the effects of burial rate and burial time; (4) To identify potential discontinuities that may be candidates for décollement positions; (5) To identify any thermal history indicators and any effects of early diagenesis; (6) To identify fluid sources and changes with depth; (7) To determine the composition and origin of basement at the site and its effect on overlying sediments; and (8) To compare the lithostratigraphy, geochemistry, and physical/mechanical properties with those at Site U1480 to establish local variations of the stratigraphic succession.

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          The least-squares line and plane and the analysis of palaeomagnetic data

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            A Paleolatitude Calculator for Paleoclimate Studies

            Realistic appraisal of paleoclimatic information obtained from a particular location requires accurate knowledge of its paleolatitude defined relative to the Earth’s spin-axis. This is crucial to, among others, correctly assess the amount of solar energy received at a location at the moment of sediment deposition. The paleolatitude of an arbitrary location can in principle be reconstructed from tectonic plate reconstructions that (1) restore the relative motions between plates based on (marine) magnetic anomalies, and (2) reconstruct all plates relative to the spin axis using a paleomagnetic reference frame based on a global apparent polar wander path. Whereas many studies do employ high-quality relative plate reconstructions, the necessity of using a paleomagnetic reference frame for climate studies rather than a mantle reference frame appears under-appreciated. In this paper, we briefly summarize the theory of plate tectonic reconstructions and their reference frames tailored towards applications of paleoclimate reconstruction, and show that using a mantle reference frame, which defines plate positions relative to the mantle, instead of a paleomagnetic reference frame may introduce errors in paleolatitude of more than 15° (>1500 km). This is because mantle reference frames cannot constrain, or are specifically corrected for the effects of true polar wander. We used the latest, state-of-the-art plate reconstructions to build a global plate circuit, and developed an online, user-friendly paleolatitude calculator for the last 200 million years by placing this plate circuit in three widely used global apparent polar wander paths. As a novelty, this calculator adds error bars to paleolatitude estimates that can be incorporated in climate modeling. The calculator is available at www.paleolatitude.org. We illustrate the use of the paleolatitude calculator by showing how an apparent wide spread in Eocene sea surface temperatures of southern high latitudes may be in part explained by a much wider paleolatitudinal distribution of sites than previously assumed.
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              Physical properties of seawater: A new salinity scale and equation of state for seawater

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                Author and article information

                Journal
                10.14379/iodp.proc.362.2017
                Proceedings of the International Ocean Discovery Program
                International Ocean Discovery Program
                2377-3189
                06 October 2017
                Article
                10.14379/iodp.proc.362.104.2017
                185c80cb-3a1e-4b8a-a94f-7e839b84a996

                This work is licensed under a Creative Commons Attribution 4.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/

                History

                Earth & Environmental sciences,Oceanography & Hydrology,Geophysics,Chemistry,Geosciences

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